
doi: 10.1063/1.1662218
Fused quartz capillaries 700 and 1200 m long and 100 μm in inside diameter have been filled under hydrostatic pressure. It is verified that the rate of filling is governed by Poiseuille's law, which predicts the filled length to be proportional to the square root of the filling time. At a pressure of 270 atm, 250 m was filled in 1 h, 800 m in 10 h, and 1200 m in 21 h. The filling rate cannot be increased significantly from the above values by increasing the pressure because of the increase in the viscosity of the fluid with increasing pressure. Since it requires high pressure to move the liquid in a long capillary, it is apparent that liquid will not flow out of a long capillary that is not under pressure.
| selected citations These citations are derived from selected sources. This is an alternative to the "Influence" indicator, which also reflects the overall/total impact of an article in the research community at large, based on the underlying citation network (diachronically). | 2 | |
| popularity This indicator reflects the "current" impact/attention (the "hype") of an article in the research community at large, based on the underlying citation network. | Average | |
| influence This indicator reflects the overall/total impact of an article in the research community at large, based on the underlying citation network (diachronically). | Average | |
| impulse This indicator reflects the initial momentum of an article directly after its publication, based on the underlying citation network. | Average |
